Venus Origins Explorer (VOX) concept: A proposed new frontiers mission

Of all known planets and moons in the galaxy, Venus remains the most Earth-like in terms of size, composition, surface age, and distance from the Sun [1]. Although not currently habitable, Venus lies within the Sun's ‘Goldilocks zone’, and may have been habitable before Earth [2]. What caused Venus to follow a divergent path to its present hostile environment, devoid of oceans, magnetic field, and plate tectonics that have enabled Earth's long-term habitability? The proposed Venus Origins Explorer (VOX) would determine how the evolution of Earth's twin diverged, and enable breakthroughs in our understanding of terrestrial planet evolution and habitability in our own solar system — and others. The VOX mission concept consists of two flight elements: 1) an Atmosphere Sampling Vehicle (ASV), and 2) an Orbiter that accommodates the ASV and also provides global reconnaissance of Venus using just two instruments and a gravity science investigation. The ASV would be released shortly after Venus Orbit Insertion and dips into the well-mixed atmosphere at 112 km. It delivers an in situ atmospheric sample to the Venus Original Constituents Experiment (VOCE) to measure noble gases, revealing the source and evolution of Venus' volatiles. The Orbiter uses the Venus Emissivity Mapper (VEM) to map global surface mineralogy and search for active or recent volcanism. Venus Interferometric Synthetic Aperture Radar (VISAR) generates long-awaited high-resolution imaging and digital elevation models, and possible deformation maps with repeat-pass interferometry, a new tool for planetary science. Ka-band tracking increases the gravity field resolution, enabling global elastic thickness estimates. Using a low risk implementation and just three instruments plus gravity science, VOX conducts a comprehensive global investigation of Venus' dynamic surface. As described below, VOX meets and exceeds the science objectives prescribed in the National Academy of Sciences most recent Planetary Science Decadal Survey. VOX is the logical next mission to Venus because it: 1) addresses top priority atmosphere, surface, and interior science objectives; 2) produces key global datasets to enable comparative planetology; 3) provides high-resolution global topography, composition, and imaging necessary to optimize future landed missions; 4) creates opportunities for revolutionary discoveries and observations of ongoing Venus geological activity, over a three-year period from an orbital platform plus an in situ atmospheric sampling vehicle; and 5) fuels the next generation of scientists by providing 44 Tb of science data. Additionally, VOX offers NASA the ability to select and fly small sats at Venus by providing relay and the ability to trade aerobraking duration for additional mass capability.

[1]  Mario D'Amore,et al.  Idunn Mons on Venus: Location and extent of recently active lava flows , 2017 .

[2]  Franck Montmessin,et al.  Variations of sulphur dioxide at the cloud top of Venus’s dynamic atmosphere , 2012, Nature Geoscience.

[3]  Martha S. Gilmore,et al.  VIRTIS emissivity of Alpha Regio, Venus, with implications for tessera composition , 2015 .

[4]  Giuseppe Piccioni,et al.  Venus surface thermal emission at 1 μm in VIRTIS imaging observations: Evidence for variation of crust and mantle differentiation conditions , 2008 .

[5]  N. Toomarian,et al.  On-Orbit Measurements of the ISS Atmosphere by the Vehicle Cabin Atmosphere Monitor , 2011 .

[6]  S. Smrekar,et al.  Experimental and observational evidence for plume-induced subduction on Venus , 2017 .

[7]  Oleg Korablev,et al.  Atmospheric chemistry suite (ACS): a set of infrared spectrometers for atmospheric measurements on board ExoMars trace gas orbiter , 2013, Optics & Photonics - Optical Engineering + Applications.

[8]  P. Drossart,et al.  Recent Hotspot Volcanism on Venus from VIRTIS Emissivity Data , 2010, Science.

[9]  Giuseppe Piccioni,et al.  Surface brightness variations seen by VIRTIS on Venus Express and implications for the evolution of the Lada Terra region, Venus , 2008 .

[10]  David Kappel,et al.  Radiative energy balance of Venus: An approach to parameterize thermal cooling and solar heating rates , 2017 .

[11]  B. Marty,et al.  Origins of volatile elements (H, C, N, noble gases) on Earth and Mars in light of recent results from the ROSETTA cometary mission , 2016 .

[12]  D. Nikolić,et al.  Accurate Xe Isotope Measurement Using JPL Ion Trap , 2014, Journal of The American Society for Mass Spectrometry.

[13]  D. Vokrouhlický,et al.  On Asteroid Impacts, Crater Scaling Laws, and a Proposed Younger Surface Age for Venus , 2016 .

[14]  Ann Carine Vandaele,et al.  Update of the Venus density and temperature profiles at high altitude measured by SOIR on board Venus Express , 2015 .

[15]  Bernard Marty The origins and concentrations of water, carbon, nitrogen and noble gases on Earth , 2012 .

[16]  A. Johansen,et al.  Fossilized condensation lines in the Solar System protoplanetary disk , 2015, 1511.06556.

[17]  Dimitar Sasselov,et al.  MASS–RADIUS RELATION FOR ROCKY PLANETS BASED ON PREM , 2015, 1512.08827.

[18]  E. A. Mason,et al.  TEMPERATURE DEPENDENCE OF GASEOUS DIFFUSION COEFFICIENTS , 1980 .

[19]  Robert R. Herrick,et al.  Postimpact modification by volcanic or tectonic processes as the rule, not the exception, for Venusian craters , 2011 .

[20]  David Kappel,et al.  Multi-spectrum retrieval of Venus IR surface emissivity maps from VIRTIS/VEX nightside measurements at Themis Regio , 2016 .

[21]  Seiji Sugita,et al.  On observing the compositional variability of the surface of Venus using nightside near‐infrared thermal radiation , 2003 .

[22]  Thomas Widemann,et al.  The Venus Emissivity Mapper (VEM) concept , 2016, Optical Engineering + Applications.

[23]  E. Rodríguez,et al.  Theory and design of interferometric synthetic aperture radars , 1992 .

[24]  Fuk K. Li,et al.  Synthetic aperture radar interferometry , 2000, Proceedings of the IEEE.

[25]  T. Spohn,et al.  Biotic vs abiotic Earth: A model for mantle hydration and continental coverage , 2014 .

[26]  W. Sjogren,et al.  Magellan ephemeris improvement using synthetic aperture radar landmark measurements , 1992 .

[27]  Giuseppe Piccioni,et al.  Rotation period of Venus estimated from Venus Express VIRTIS images and Magellan altimetry , 2012 .

[28]  David Kappel,et al.  MSR, a multi-spectrum retrieval technique for spatially-temporally correlated or common Venus surface and atmosphere parameters , 2014 .

[29]  Suzanne E. Smrekar,et al.  Search for active lava flows with VIRTIS on Venus Express , 2012 .

[30]  A. Treiman Geochemistry of Venus' Surface: Current Limitations as Future Opportunities , 2013 .

[31]  Giuseppe Piccioni,et al.  Refinements in the data analysis of VIRTIS-M-IR Venus nightside spectra , 2012 .

[32]  D. Pinti The Origin and Evolution of the Oceans , 2005 .

[33]  D. Campbell,et al.  Pyroclastic flow deposits on Venus as indicators of renewed magmatic activity , 2017, Journal of geophysical research. Planets.

[34]  Jean Souchay,et al.  The various contributions in Venus rotation rate and LOD , 2011 .

[35]  Maxwell Kelley,et al.  Was Venus the First Habitable World of our Solar System? , 2016, Geophysical research letters.

[36]  R. Clancy,et al.  The thermal structure of the Venus atmosphere: Intercomparison of Venus Express and ground based observations of vertical temperature and density profiles , 2017 .

[37]  V. I. Moroz,et al.  Estimates of visibility of the surface of Venus from descent probes and balloons , 2002 .

[38]  Ann Carine Vandaele,et al.  Densities and temperatures in the Venus mesosphere and lower thermosphere retrieved from SOIR on board Venus Express: Carbon dioxide measurements at the Venus terminator , 2012 .